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首页> 外文期刊>Mediterranean Marine Science >Preliminary assessment of methanogenic microbial communities in marine caves of Zakynthos Island (Ionian Sea, Greece)
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Preliminary assessment of methanogenic microbial communities in marine caves of Zakynthos Island (Ionian Sea, Greece)

机译:扎金索斯岛(希腊爱奥尼亚海)海洋洞穴中产甲烷微生物群落的初步评估

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Mediterranean marine caves remain largely unexplored, while particularly limited information is available about the microbial life existing in these unique environments. The present study is a preliminary assessment of the composition of the active anaerobic microbial community colonizing the walls of newly explored systems of underwater caves and small cavities in Zakynthos Island. The interior of these caves is densely coated with egg-shaped, foam-shaped and filamentous biological structures that are characterised by a strong odor of hydrogen sulfide gas. A total of twelve structures scrapped from cave rocks were subjected to anaerobic cultivation for up to 208 days. Strong to moderate methanogenesis was observed in two different types of egg-shaped structures and one foam-like structure. Interestingly, this was observed in experiments that were performed at room temperature (i.e. 25 o C) which is substantially lower than those typically considered optimum for methane production (e.g. 35 o C). Analysis of the 16S rRNA genes revealed a clear dominance of archaea and bacteria closely related to known methane producers and sulfate reducers, including members of the families Methanomicrobiaceae, Desulfobulbaceae , Desulfobacteraceae , Desulfuromonaceae , Campylobacteraceae , Marinifilaceae , Clostridiaceae , Incertae Sedis – Family I & II. These results show that Mediterranean marine caves can host members of archaea and bacteria with potential biotechnological interest that deserve further investigation.
机译:地中海海洋洞穴在很大程度上仍未开发,而有关这些独特环境中存在的微生物生命的信息特别有限。本研究是对活跃的厌氧微生物群落组成的初步评估,该群落遍布在扎金索斯岛的新发现的水下洞穴和小洞穴系统的壁上。这些洞穴的内部密集地覆盖着蛋形,泡沫状和丝状生物结构,其特征在于强烈的硫化氢气体气味。从洞穴岩石报废的总共十二个结构进行厌氧培养长达208天。在两种不同类型的蛋形结构和一种泡沫状结构中观察到强到中等的产甲烷作用。有趣的是,这是在室温(即25 o C)下进行的实验中观察到的,该温度大大低于通常认为对甲烷生产最适宜的温度(例如35 o C)。对16S rRNA基因的分析显示,古细菌和细菌与已知的甲烷生产者和硫酸盐还原剂密切相关,其中包括甲烷微生物菌科,脱硫鳞茎科,脱硫细菌科,脱硫呋喃葡萄科,弯曲杆菌科,马里尼菲科,梭菌科,,科。这些结果表明,地中海海洋洞穴可以容纳具有潜在生物技术价值的古细菌和细菌成员,值得进一步研究。

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